Weather Alert in Kansas
Flash Flood Warning issued August 28 at 6:27AM CDT until August 28 at 10:30AM CDT by NWS Wichita KS
AREAS AFFECTED: Chautauqua, KS; Montgomery, KS
DESCRIPTION: FFWICT The National Weather Service in Wichita has issued a * Flash Flood Warning for... Northeastern Chautauqua County in southeastern Kansas... Southern Montgomery County in southeastern Kansas... * Until 1030 AM CDT. * At 627 AM CDT, Doppler radar indicated thunderstorms producing heavy rain across the warned area. Up to 5 inches of rain have fallen. Additional rainfall amounts up to 2 inches are possible in the warned area through this morning. Flash flooding is possible. HAZARD...Life threatening flash flooding. Thunderstorms producing flash flooding. SOURCE...Radar. IMPACT...Life threatening flash flooding of creeks and streams, urban areas, highways, streets and underpasses. * Some locations that may experience flash flooding include... Coffeyville, Independence, Caney, Dearing, Elk City, Tyro, Havana, Bolton, Independence Airport, Elk City Lake, Elk City State Park and Hale.
INSTRUCTION: Do not drive into flooded areas or go around barricades. Nearly two feet of water will carry most vehicles away. Turn around, don't drown.
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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